Late Paleozoic rock deformation of the Kurai block: Structural-kinematic analysis (upper Kuraika River, Gorny Altai, Russia)

dc.contributor.author	Abildaeva M.
dc.contributor.author	Zinoviev S.
dc.contributor.author	Buslov M.
dc.date.accessioned	2020-01-15T22:01:57Z
dc.date.available	2020-01-15T22:01:57Z
dc.date.issued	2019
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/156525
dc.description.abstract	© 2019 Institute of the Earth's Crust. All rights reserved. In the Kurai ridge located in the southeastern Gorny Altai (Altai Mountains, Russia) metamorphic rocks of the Kurai complex are widely developed: granite-gneisses, crystalline schists and amphibolites, including widespread Early Carboniferous mylonites and blastomylonites. Oriented samples of blastomylonites were taken from the upper reaches of the Kuraika river for the microstructural study aimed to determine the kinematics of movements. The analyses of thin cut samples show structural-kinematic indicators that suggest two deformation events (left-lateral shearing, then right-lateral shearing).
dc.subject	Blastomylonite
dc.subject	Fold-nappe structure
dc.subject	Kinematic analysis
dc.subject	Kurai metamorphic complex
dc.subject	Strike-slip fault
dc.title	Late Paleozoic rock deformation of the Kurai block: Structural-kinematic analysis (upper Kuraika River, Gorny Altai, Russia)
dc.type	Article
dc.relation.ispartofseries-issue	4
dc.relation.ispartofseries-volume	10
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	937
dc.source.id	SCOPUS-2019-10-4-SID85076613950

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